渤海湾盆地黄骅坳陷中北区新生代幕式沉降过程

祁鹏; 任建业; 卢刚臣; 史双双; 佟殿君; 张俊霞

doi:10.3799/dqkx.2010.118

Volume 35 Issue 6

Jun. 2010

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Article Navigation > Earth Science > 2010 > 35(6): 1041-1052

QI Peng, REN Jian-ye, LU Gang-chen, SHI Shuang-shuang, TONG Dian-jun, ZHANG Jun-xia, 2010. Cenozoic Episodic Subsidence in the Middle and North Part of Huanghua Depression, Bohai Bay Basin. Earth Science, 35(6): 1041-1052. doi: 10.3799/dqkx.2010.118

Citation:

QI Peng, REN Jian-ye, LU Gang-chen, SHI Shuang-shuang, TONG Dian-jun, ZHANG Jun-xia, 2010. Cenozoic Episodic Subsidence in the Middle and North Part of Huanghua Depression, Bohai Bay Basin. Earth Science, 35(6): 1041-1052. doi: 10.3799/dqkx.2010.118

Citation:

QI Peng, REN Jian-ye, LU Gang-chen, SHI Shuang-shuang, TONG Dian-jun, ZHANG Jun-xia, 2010. Cenozoic Episodic Subsidence in the Middle and North Part of Huanghua Depression, Bohai Bay Basin. Earth Science, 35(6): 1041-1052. doi: 10.3799/dqkx.2010.118

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Cenozoic Episodic Subsidence in the Middle and North Part of Huanghua Depression, Bohai Bay Basin

doi: 10.3799/dqkx.2010.118

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Secondary Center of CUG, Structural Research Center of Oil & Gas Bearing Basin, Ministry of Education, Wuhan 430074, China
4.
Dagang Sub-division of GRI, BGP, Tianjin 300280, China
5.
Faculty of Economics and Management, China University of Geosciences, Wuhan 430074, China

Received Date: 2010-03-21
Publish Date: 2010-11-01

Abstract

Abstract

The middle and north area of Huanghua depression, located in the middle of the Bohai Bay basin, is a significant Cenozoic tectonic unit. This study area underwent the episodic subsidence and the subsidence center migrated regularly which was interpreted through the analysis of the tectonic-sequence surface, syn-sedimentary fault's activity and the back-stripping of the subsidence history. The bottom interface of Guantao Formation is a regional post-rifting unconformity surface and divides the basin's Cenozoic evolution into rifting and post-rifting stage. In the filling sequence of the rifting stage, the bottom interface of the first member of Shahejie Formation is also a regional recognizable angle disconformity surface in the whole basin and divides the rifting stage into Episodic Ⅰ and Episodic Ⅱ. The geometry feature and property of the fault system shows that the tectonic deformation of the study area was controlled by the NW-SE extending stress field in the rifting Episodic Ⅰ from Es₃ to Es₂. However, the extending stress field turned to NS in the Episodic Ⅱ from Es₁ to Ed. In the post-rifting stage, the middle and north area of Huanghua depression underwent stable subsidence at early stage and accelerated subsidence at late stage. This episodic subsidence process is closely related to the change of the regional extending stress field orientation which was controlled by the tectonic events of the surrounding plates. Especially, the accelerated westward subduction from the Pacific Plate to the Eurasia Plate triggered the southward expanding of the dextral slipping of the Tanlu fault and the activity of the north section of the Lanliao fault through the Huanghua depression after the Late Eocene. The continued dextral slipping between the east and west boundary faults created a NS trending extensional overlap at the Bohai Sea, completely changed the stress field distribution in the middle and north area of Huanghua depression, and generated the episodic evolution in the rifting stage.
- Huanghua depression,
- episodic subsidence,
- Cenozoic,
- tectonics

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References(49)

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Cenozoic Episodic Subsidence in the Middle and North Part of Huanghua Depression, Bohai Bay Basin

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